MCST – MODLAND

Eric F. Vermote –MODLAND representative

Organization

• MODLAND is working with MCST through bi-weekly meeting MSWG (Z. Wan, E. Vermote)

• E. Vermote have ad-hoc interactions with MCST through dedicated Point of Contact (Vincent Chiang)

Issues being tracked• Reflective bands calibration accuracy and stability

(comparison Aqua-Terra on desert sites shows agreement 1-2%) band 1 and 2 – Green

• Striping in Terra SWIR (esp. Band7), several methods are being evaluated (eliminating noisy detector, atmosphere de-striping, Xtalk correction – MCST) –Yellow

• Band to Band registration Aqua YellowTerra Green• Polarization correction/RVS to be used for aerosol

inversion over Land at 412nm (characterization has been provided by MCST) – Yellow

• LWIR and MWIR performances (S. Hook) Green/Yellow

Independent reflectance calibration accuracy assessment

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MCST ratio preflight to solar diffuser calibration

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Terra band 1 and band 2 directional surface reflectance

Terra band 1 and band 2 surface reflectance normalized for BRDF at nadir view and solar zenith angle of 45 degrees.

Terra NDVI computed from band 1 and band 2 surface reflectance normalized for BRDF at nadir view and solar

zenith angle of 45 degrees.

Aqua band 1 and band 2 surface reflectance normalized for BRDF at nadir view and solar zenith angle of 45 degrees.

Aqua NDVI computed from band 1 and band 2 surface reflectance normalized for BRDF at nadir view and solar

zenith angle of 45 degrees.

Comparison of Terra and Aqua band1

1.2%3%

Comparison of Terra and Aqua band2

1.6%0.6%

Band 1 smooth data

Band 2 smooth data

Band 1 Terra-Aqua

Band 2 Terra-Aqua

NDVI Terra-Aqua

Conclusion

• Could be a systematic difference between Aqua and Terra due to overpass time (10h30 versus 1h30pm)

De stripping evaluation (Terra)

Test granule

- Compare original data to:

-the fix in surface reflectance (ignoring some noisy detector in band 7)-The de-stripped Level 1B provided by atmosphere

original Fix Using B7 destriped

B7 original

The improvement by the “fix” is still showing stripes (but reduced),The version using the Level 1B de-strippedprovided by atmosphere does not showany stripe.

Overall the impact of using destriped L1B is less than 0.005 in band 1 (less than quoted accuracy)for the cloud free pixels

Pixels with change >0.005 in band 1 aremasked in Magenta

The performance of de-striping is very good over uniform areas

1(red), 4 (green), 3(blue) Band 7 (original)

original

Band 7 (original-destriped)

Conclusion

• The atmosphere destriping algorithm has been sucessfully used in land collection 5 and will be used in collection 6.

MODIS/Aqua Band-to-band Registration Performance

Source: MODIS ST Meeting – Calibration Workshop, J. Xiong, March 2005 (slide 31)

VIS VISNIR NIRS/MWIR S/MWIR LWIRBand

Misregistration on 500m bands

Reflectance transect alongTrack on a L1B subset

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Impact on the aerosol product (relationship band 3 band 7)

band 3 and band 7 are plottedagainst each other in the sub area inside the magenta box

Shifting one row (500m) improves the correlation (from 0.85 to 0.94) decreases the Standard deviation (from 0.018 to 0.012) and has a impact on the slope (used in the aerosol retrieval)

Aqua BBR fixes

• Software fixes (shifting 1row and accounting for earth rotation) has been performed along track to improve the band to band registration of bands 5-6-7 with bands 1,2,3,4 prior to aerosol retrieval

Polarization effect at 412nm depending on mirror side for

Terra (band 8)

• Pbs detected over the rain forest at high aerosol level (between 0.8-1.2): band 8 noise make the aerosol model switch to high to low absorption

Band 8/ Band 8 details

Terra, Band 8 (412nm) Mirror side calibration artifact

Surface reflectance in band 8, changing From +0.007 to -0.003 over a forest area in south America.

Mirror side effect in Terra band 8 despite mirror side equalization also visible over snow/ice target

(polar zone)

This is not apparent on Aqua data

Terra Mirror side ratio is dependent on AOI (fine) but Australian and Lybian desert give different ratio at EDGE

AOI

Polarization simulation over desert sites may explain the previous results: The polarization over

Lybia and Australia are out of phase

Conclusion on polarization

• Need to implement polarization correction for Terra especially since 2005 (went up from 5% to 30%)

MCST – MODLAND OrganizationIssues being trackedIndependent reflectance calibration accuracy assessmentTerra band 1 and band 2 directional surface reflectanceSlide Number 6Slide Number 7Slide Number 8Slide Number 9Comparison of Terra and Aqua band1Comparison of Terra and Aqua band2Band 1 smooth dataBand 2 smooth dataBand 1 Terra-AquaBand 2 Terra-AquaNDVI Terra-AquaConclusionDe stripping evaluation (Terra)Slide Number 19Slide Number 20Slide Number 21Conclusion MODIS/Aqua Band-to-band Registration PerformanceMisregistration on 500m bandsImpact on the aerosol product (relationship band 3 band 7)Aqua BBR fixesPolarization effect at 412nm depending on mirror side for Terra (band 8)Slide Number 28Band 8/ Band 8 detailsTerra, Band 8 (412nm) Mirror side calibration artifactMirror side effect in Terra band 8 despite mirror side equalization also visible over snow/ice target (polar zone)This is not apparent on Aqua dataTerra Mirror side ratio is dependent on AOI (fine) but Australian and Lybian desert give different ratio at EDGE AOIPolarization simulation over desert sites may explain the previous results: The polarization over Lybia and Australia are out of phaseConclusion on polarization